The Dust Environment of Comet 67P/Churyumov-Gerasimenko

Total Page:16

File Type:pdf, Size:1020Kb

The Dust Environment of Comet 67P/Churyumov-Gerasimenko A&A 422, 357–368 (2004) Astronomy DOI: 10.1051/0004-6361:20035806 & c ESO 2004 Astrophysics The dust environment of comet 67P/Churyumov-Gerasimenko M. Fulle1, C. Barbieri2,G.Cremonese3,H.Rauer4, M. Weiler4, G. Milani5, and R. Ligustri6 1 INAF - Osservatorio Astronomico di Trieste, Via Tiepolo 11, 34131 Trieste, Italy 2 Dipartimento di Astronomia, Universit`a di Padova, Vicolo dell’Osservatorio 2, 35122 Padova, Italy 3 INAF - Osservatorio Astronomico di Padova, Vicolo dell’Osservatorio 5, 35122 Padova, Italy 4 Institute of Planetary Research, DLR Rutherfordstrasse 2, 12849 Berlin, Germany 5 Unione Astrofili Italiani, UAI 6 Osservatorio di Talmassons, CAST, Talmassons (Ud), Italy Received 4 December 2003 / Accepted 6 April 2004 Abstract. The new target of the ESA Rosetta Mission is comet 67P/Churyumov-Gerasimenko, which passed its last perihelion on 18 August 2002 and was well observed from fall 2002 to spring 2003. Its most prominent feature was a thin dust tail, which is best fitted by the Neck-Line model. Fits of the whole tail provide the dust environment of 67P during a year around perihelion; it shows a strong asymmetry between pre and post perihelion times. The dust mass loss rate appears constant since 2 AU before perihelion at about 200 kg s−1, a factor 100 higher than 46P/Wirtanen, the previous Rosetta target. Neck-Line photometry during 2002 and 2003 suggests that such a dust environment has remained similar since 3.6 AU before perihelion, i.e. the distance at which Rosetta science operations will start and the lander will be delivered to the surface. Key words. space vehicles – comets: general – comets: individual: 67P/Churyumov-Gerasimenko 1. Introduction observability after the perihelion passage of August 18, 2002: before August 2002 and after spring 2003, the comet was too Due to a launch delay, in February 2003 ESA changed the tar- close to the Sun to be observable. We will analyse in another get of the Rosetta Mission (ESA 2003): from 46P/Wirtanen paper the data collected before the 1996 perihelion passage. to 67P/Churyumov-Gerasimenko (67P hereafter for brevity). During 2002 and 2003, 67P showed a 10 arcmin long and thin A strong effort was required to obtain information on the new tail (Fig. 1), bright enough to be monitored by CCD cameras of target in order to change the orbiting strategies to adapt the al- amateur astronomers. This is unusual for short-period comets, ready built spacecraft and instruments to an environment pos- which rarely show bright tails. We will show in this paper that, sibly different from the planned one: this regards not only the certainly during all spring 2003, and probably also during fall shape and size of the nucleus, but also the coma environment, 2002, this tail was a dust tail. If ground-based observations only which is related to shape and spin state of the nucleus. Here we are available, models of dust tails provide the most complete focus on the dust environment of 67P: a comparison with the information on a comet dust environment (Fulle 1999). Coma environment of the previous target 46P will allow us to outline photometry, quantified by the quantity Afρ (A’Hearn et al. the differences between two well studied short-period comets, 1984), will then be used to constrain the outputs of dust tail in order to understand if 67P is representative of the family of models. These suggest that the dust environment of 67P may short-period comets. Moreover, a model of the dust environ- be different from that of typical short-period comets, in which ment is necessary to plan the operations of the many instru- such a long lasting dust tail was never observed. Therefore, a ments studying the dust ejected from the comet, to determine deep analysis of the dust environment of 67P is even more im- the orbiting strategies, the software robustness of the naviga- portant in the perspective of the Rosetta Mission. tion cameras against false nucleus detection, and the lifetime Let us recall that one of the difficulties in interpreting dust of the landing probe against dust pollution. images is that the dust ejections occurring days before, months In this paper we consider IRAS observations performed before or years before the time of observation form patterns in 1983 (Sykes & Walker 1992) and ground-based data col- which may have a similar appearance. Therefore, extreme care lected on the dust ejected from 67P during the nine months of must be paid to obtain a correct identification. If an observed Send offprint requests to: M. Fulle, e-mail: [email protected] pattern is improperly identified, the derived time (and in gen- Based also on observations collected at the National Galileo eral the rate) of dust production will be severely in error. In Telescope and the 2 m telescope of the Th¨uringer Landessternwarte the case of 67P, the identification of the thin tail in terms of Tautenburg. a trail (Sykes & Walker 1992) or in terms of a Neck-Line Article published by EDP Sciences and available at http://www.aanda.org or http://dx.doi.org/10.1051/0004-6361:20035806 358 M. Fulle et al.: The dust environment of comet 67P/Churyumov-Gerasimenko Table 1. The observed Position Angle PAT of the Tail is compared with the antisolar direction (Position Angle PARV of the prolonged radius vec- tor) and the expected position of the dust trail (Position Angle PACO of the comet orbit projected on the sky). The observed PAT values are best fit by the computed PANL of the Neck-Line ejected at Sun-Comet distances r(θ−π)andatthet(θ−π)−T times (days with respect to perihelion T), where θ is the comet true anomaly at observation. Observers: DT, Diego Tirelli; RL, Rolando Ligustri (Talmassons Observatory); HM, Hermann Mikuz (Crni Vrh Observatory); TNG, National Galileo Telescope; TLS, Tautenburg Schmidt Telescope at Th¨uringer LandesSternwarte. Time UT t(θ) − Tr(θ) θ t(θ − π) − Tr(θ − π)PANL PA CO PA RV PA T Band Observer [days] [AU] [◦] [days] [AU] [◦][◦][◦][◦] 14.094 Aug. 2002 –4.219 1.29 –3.6 – – – 263.7 272.4 270 ± 3 R RL 8.107 Sep. 2002 21.794 1.32 18.4 –810 5.28 275.4 274.6 283.3 280 ± 3 V DT 19.134 Oct. 2002 62.821 1.49 48.4 –378 3.62 289.8 288.6 293.5 290 ± 3 V DT 8.059 Nov. 2002 82.746 1.61 60.7 –285 3.05 294.2 293.9 295.0 294 ± 3 R RL 11.154 Nov. 2002 85.841 1.63 62.4 –275 2.99 294.7 294.6 295.1 296 ± 3 V DT 4.175 Jan. 2003 140.862 2.03 86.3 –164.2 2.20 299.3 303.9 291.0 296 ± 3 V DT 11.188 Jan. 2003 147.875 2.08 88.7 –156.4 2.14 299.3 304.3 289.6 297 ± 3 R RL 12.197 Jan. 2003 148.884 2.09 89.0 –155.3 2.13 299.3 304.4 289.4 295 ± 3 R RL 2.003 Feb. 2003 167.690 2.23 94.8 –138.0 2.00 298.6 303.9 282.7 297 ± 3 R RL 22.935 Mar. 2003 216.622 2.58 107.0 –107.7 1.78 294.6 297.6 138.7 296 ± 2 R HM 27.000 Mar. 2003 220.687 2.61 107.8 –105.8 1.77 294.4 297.1 133.2 294.5 ± 0.5 R TNG 27.875 Mar. 2003 221.562 2.62 108.0 –105.4 1.76 294.3 297.0 132.2 294.0 ± 0.5 R TLS 28.028 Mar. 2003 221.715 2.62 108.1 –105.3 1.76 294.3 297.0 132.0 294.0 ± 0.5 R TLS 28.896 Mar. 2003 222.583 2.63 108.2 –104.9 1.76 294.3 296.9 131.1 294.0 ± 0.5 R TLS 6.922 Apr. 2003 230.609 2.69 110.1 –101.0 1.73 294.0 296.2 124.5 294 ± 2 R HM 2. 67P Tail: Evolution over nine months Databases of the Comet Section of the Italian Amateur Astronomer Union (UAI) contain many CCD images following the evolution of the thin tail during the whole 2002/03 observ- ability window (UAI 2003). These images are filtered using broadband filters only, like Cousins R, and are here comple- mented by four images of much higher quality obtained at the National Galileo Telescope and the Tautenburg Schmidt Telescope (Weiler et al. 2004a, Fig. 1). The log of all the ob- servations analysed in this paper is reported in Table 1. Here we report also the correspondence among UT times, the comet true anomaly θ (i.e. the angle between the Sun-Comet and the Sun-perihelion vectors), the observation time related to perihe- Fig. 1. Image of the thin tail of 67P taken on 27.875 March 2003 UT lion t(θ) − T, and the Sun-Comet distance r(θ): in the following at the 2 m Tautenburg Schmidt Telescope (see Table 1 for details of sections and figures, Table 1 can be used to convert one of these the observations). 67P showed a similar tail during nine months af- ter 2002 perihelion. The axis units are pixels, with scale 1.23 arc- quantities to the others. sec pixel−1 (the scale reported in Weiler et al. (2004a) is wrong). The The 67P tail is so thin that it can be described as a image width is 9×105 km projected at the Earth-comet distance.
Recommended publications
  • 1 Characterization of Cometary Activity of 67P/Churyumov-Gerasimenko
    Characterization of cometary activity of 67P/Churyumov-Gerasimenko comet Abstract After 2.5 years from the end of the mission, the data provided by the ESA/Rosetta mission still leads to important results about 67P/Churyumov-Gerasimenko (hereafter 67P), belonging to the Jupiter Family Comets. Since comets are among the most primitive bodies of the Solar System, the understanding of their formation and evolution gives important clues about the early stages of our planetary system, including the scenarios of water delivery to Earth. At the present state of knowledge, 67P’s activity has been characterized by measuring the physical properties of the gas and dust coma, by detecting water ice patches on the nucleus surface and by analyzing some peculiar events, such as outbursts. We propose an ISSI International Team to build a more complete scenario of the 67P activity during different stages of its orbit. The retrieved results in terms of dust emission, morphology and composition will be linked together in order to offer new insights about 67P formation and evolution. In particular the main goals of the project are: 1. Retrieval of the activity degree of different 67P geomorphological nucleus regions in different time periods, by reconstructing the motion of the dust particles revealed in the coma; 2. Identification of the main drivers of cometary activity, by studying the link between cometary activity and illumination/local time, dust morphology, surface geomorphology, dust composition. The project will shed light on how (and if) cometary activity is related to surface geology and/or composition or is just driven by local illumination.
    [Show full text]
  • Stardust Comet Flyby
    NATIONAL AERONAUTICS AND SPACE ADMINISTRATION Stardust Comet Flyby Press Kit January 2004 Contacts Don Savage Policy/Program Management 202/358-1727 NASA Headquarters, Washington DC Agle Stardust Mission 818/393-9011 Jet Propulsion Laboratory, Pasadena, Calif. Vince Stricherz Science Investigation 206/543-2580 University of Washington, Seattle, WA Contents General Release ……………………………………......………….......................…...…… 3 Media Services Information ……………………….................…………….................……. 5 Quick Facts …………………………………………..................………....…........…....….. 6 Why Stardust?..................…………………………..................………….....………......... 7 Other Comet Missions ....................................................................................... 10 NASA's Discovery Program ............................................................................... 12 Mission Overview …………………………………….................……….....……........…… 15 Spacecraft ………………………………………………..................…..……........……… 25 Science Objectives …………………………………..................……………...…........….. 34 Program/Project Management …………………………...................…..…..………...... 37 1 2 GENERAL RELEASE: NASA COMET HUNTER CLOSING ON QUARRY Having trekked 3.2 billion kilometers (2 billion miles) across cold, radiation-charged and interstellar-dust-swept space in just under five years, NASA's Stardust spacecraft is closing in on the main target of its mission -- a comet flyby. "As the saying goes, 'We are good to go,'" said project manager Tom Duxbury at NASA's Jet
    [Show full text]
  • Dust-To-Gas and Refractory-To-Ice Mass Ratios of Comet 67P
    Dust-to-Gas and Refractory-to-Ice Mass Ratios of Comet 67P/Churyumov-Gerasimenko from Rosetta Observations Mathieu Choukroun, Kathrin Altwegg, Ekkehard Kührt, Nicolas Biver, Dominique Bockelée-Morvan, Joanna Drążkowska, Alain Hérique, Martin Hilchenbach, Raphael Marschall, Martin Pätzold, et al. To cite this version: Mathieu Choukroun, Kathrin Altwegg, Ekkehard Kührt, Nicolas Biver, Dominique Bockelée-Morvan, et al.. Dust-to-Gas and Refractory-to-Ice Mass Ratios of Comet 67P/Churyumov-Gerasimenko from Rosetta Observations. Journal Space Science Reviews, 2020, 10.1007/s11214-020-00662-1. hal- 03021621 HAL Id: hal-03021621 https://hal.archives-ouvertes.fr/hal-03021621 Submitted on 29 Aug 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution| 4.0 International License Space Sci Rev (2020) 216:44 https://doi.org/10.1007/s11214-020-00662-1 Dust-to-Gas and Refractory-to-Ice Mass Ratios of Comet 67P/Churyumov-Gerasimenko from Rosetta Observations Mathieu Choukroun1 · Kathrin Altwegg2 · Ekkehard Kührt3 · Nicolas Biver4 · Dominique Bockelée-Morvan4 · Joanna Dra˙ ˛zkowska5 · Alain Hérique6 · Martin Hilchenbach7 · Raphael Marschall8 · Martin Pätzold9 · Matthew G.G.T. Taylor10 · Nicolas Thomas2 Received: 17 May 2019 / Accepted: 19 March 2020 / Published online: 8 April 2020 © The Author(s) 2020 Abstract This chapter reviews the estimates of the dust-to-gas and refractory-to-ice mass ratios derived from Rosetta measurements in the lost materials and the nucleus of 67P/Churyumov-Gerasimenko, respectively.
    [Show full text]
  • Rosetta Observations of Plasma and Dust at Comet 67P
    Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 1989 Rosetta Observations of Plasma and Dust at Comet 67P FREDRIK LEFFE JOHANSSON ACTA UNIVERSITATIS UPSALIENSIS ISSN 1651-6214 ISBN 978-91-513-1070-1 UPPSALA urn:nbn:se:uu:diva-425953 2020 Dissertation presented at Uppsala University to be publicly examined on Zoom, Friday, 15 January 2021 at 13:15 for the degree of Doctor of Philosophy. The examination will be conducted in English. Faculty examiner: Dr. Nicolas André (IRAP, Toulouse, France). Online defence: https://uu-se.zoom.us/j/67552597754 Contact person for questions about participation is Prof. Mats André 0707-792072 Abstract Johansson, F. L. 2020. Rosetta Observations of Plasma and Dust at Comet 67P. Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 1989. 35 pp. Uppsala: Acta Universitatis Upsaliensis. ISBN 978-91-513-1070-1. In-situ observations of cometary plasma are not made because they are easy. The historic ESA Rosetta mission was launched in 2004 and traversed space for ten years before arriving at comet 67P/Churyumov-Gerasimenko, which it studied in unprecedented detail for two years. For the Rosetta Dual Langmuir Probe Experiment (LAP), the challenge was increased by the sensors being situated on short booms near a significantly negatively charged spacecraft, which deflects low-energy charged particles away from our instrument. To disentangle the cometary plasma signature in our signal, we create a charging model for the particular design of the Rosetta spacecraft through 3D Particle-in-Cell/hybrid spacecraft-plasma interaction simulations, which also can be applicable to similarly designed spacecraft in cold plasma environments.
    [Show full text]
  • Stardust Comet Dust Resembles Asteroid Materials 24 January 2008
    Stardust comet dust resembles asteroid materials 24 January 2008 treasure trove of stardust from other stars and other ancient materials. But in the case of Wild 2, that simply is not the case. By comparing the Stardust samples to cometary interplanetary dust particles (CP IDPs), the team found that two silicate materials normally found in cometary IDPs, together with other primitive materials including presolar stardust grains from other stars, have not been found in the abundances that might be expected in a Kuiper Belt comet like Getting into the details: Stardust impact tracks and light Wild 2. The high-speed capture of the Stardust gas gun impacts of sulfide in aerogel both display metal particles may be partly responsible; but extra beads with sulfide rims indicating that GEMS-like objects refractory components that formed in the inner in Stardust are generated by impact mixing of comet solar nebula within a few astronomical units of the dust with silica aerogel. (left) Stardust GEMS-like sun, indicate that the Stardust material resembles material and (right) light gas gun shot GEM-like material. chondritic meteorites from the asteroid belt. GEMS in cometary IDPs do not contain sulfide-rimmed metal inclusions. [Image credit: Hope Ishii, LLNL] “The material is a lot less primitive and more altered than materials we have gathered through high altitude capture in our own stratosphere from a variety of comets,” said LLNL’s Hope Ishii, lead Contrary to expectations for a small icy body, much author of the research that appears in the Jan. 25 of the comet dust returned by the Stardust mission edition of the journal, Science.
    [Show full text]
  • Interstellar Interlopers Two Recently Sighted Space Rocks That Came from Beyond the Solar System Have Puzzled Astronomers
    A S T R O N O MY InterstellarInterstellar Interlopers Two recently sighted space rocks that came from beyond the solar system have puzzled astronomers 42 Scientific American, October 2020 © 2020 Scientific American 1I/‘OUMUAMUA, the frst interstellar object ever observed in the solar system, passed close to Earth in 2017. InterstellarInterlopers Interlopers Two recently sighted space rocks that came from beyond the solar system have puzzled astronomers By David Jewitt and Amaya Moro-Martín Illustrations by Ron Miller October 2020, ScientificAmerican.com 43 © 2020 Scientific American David Jewitt is an astronomer at the University of California, Los Angeles, where he studies the primitive bodies of the solar system and beyond. Amaya Moro-Martín is an astronomer at the Space Telescope Science Institute in Baltimore. She investigates planetary systems and extrasolar comets. ATE IN THE EVENING OF OCTOBER 24, 2017, AN E-MAIL ARRIVED CONTAINING tantalizing news of the heavens. Astronomer Davide Farnocchia of NASA’s Jet Propulsion Laboratory was writing to one of us (Jewitt) about a new object in the sky with a very strange trajectory. Discovered six days earli- er by University of Hawaii astronomer Robert Weryk, the object, initially dubbed P10Ee5V, was traveling so fast that the sun could not keep it in orbit. Instead of its predicted path being a closed ellipse, its orbit was open, indicating that it would never return. “We still need more data,” Farnocchia wrote, “but the orbit appears to be hyperbolic.” Within a few hours, Jewitt wrote to Jane Luu, a long-time collaborator with Norwegian connections, about observing the new object with the Nordic Optical Telescope in LSpain.
    [Show full text]
  • Do Comets Have Chondrules and Cais? Evidence from the Leonid Meteors
    Meteoritics & Planetary Science 39, Nr 10, 1733–1740 (2004) Abstract available online at http://meteoritics.org Do comets have chondrules and CAIs? Evidence from the Leonid meteors Timothy D. SWINDLE1* and Humberto CAMPINS1, 2 1Lunar and Planetary Laboratory, University of Arizona, Tucson, Arizona 85721–0092, USA 2Department of Physics and Astronomy, University of Central Florida, Orlando, Florida 32816, USA *Corresponding author. E-mail: [email protected] (Received 10 June 2003; revision accepted 3 August 2004) Abstract–Chondrules, silicate spheres typically 0.1 to 1 mm in diameter, are the most abundant constituents in the most common meteorites falling on Earth, the ordinary chondrites. In addition, many primitive meteorites have calcium-aluminum-rich inclusions (CAIs). The question of whether comets have chondrules or CAIs is relevant to understanding what the interior of a comet is like and what a cometary meteorite might be like. In addition, one prominent model for forming chondrules and CAIs, the X-wind model, predicts their presence in comets, while most other models do not. At present, the best way to search for chondrules and CAIs in comets is through meteor showers derived from comets, in particular, the Leonid meteor shower. Evidence potentially could be found in the overall mass distribution of the shower, in chemical analyses of meteors, or in light curves. There is no evidence for a chondrule abundance in the Leonid meteors similar to that found in chondritic meteorites. There is intriguing evidence for chondrule- or CAI-sized objects in a small fraction of the light curves, but further work is required to generate a definitive test.
    [Show full text]
  • Sirius Astronomer Newsletter to Be the Most Tangible Asset of Membership in the OCA
    SIRIUS ASTRONOMER www.ocastronomers.org The Newsletter of the Orange County Astronomers August 2021 Free to members, subscriptions $12 for 12 issues Volume 48, Number 8 Ian Grove framed the Milky Way behind the Star Chaser observatory at the OCA Anza site. The image was taken with a Canon EOS T6 camera and 50mm lens. Because of the COVID-19 crisis and ongoing efforts to reduce exposure to the virus: . All in-person club events are cancelled . Use of the Anza site is discouraged Please read more about how OC Astronomers has modified its activities on page 2. Upcoming Events - free and open to the public Beginner’s class Friday,6 August at 7:30 to 9:30 PM ONLINE The topic this month will be the basics of astrophotography, presented by Kyle Coker Club Meeting Friday,13 August at 7:30 to 9:30 PM ONLINE "What's Up?": Chris Butler from OCA Main speaker: Dr. Shami Chatterjee from Cornell University who’s talk will be “Into the Void with Voyager, Pulsars, and Fast Radio Bursts” Open Spiral Bar Saturday, 14 August at 10:00 to 11:30 PM ONLINE Want to socialize? Grab your images, experiences, questions, or none and see your fellow Orange County Astronomers face-to-face. Please consult the calendar on the OCA website to RSVP (required) Response to COVID-19 Crisis COVID-19 continues to affect all our activities. All in-person club events remain cancelled through at least the summer of this year. Cancellation periods for specific events are detailed below. Please see the President’s Message for additional information.
    [Show full text]
  • Pan-STARRS)? C
    A&A 605, A56 (2017) Astronomy DOI: 10.1051/0004-6361/201731085 & c ESO 2017 Astrophysics X-shooter search for outgassing from main belt comet P/2012 T1 (Pan-STARRS)? C. Snodgrass1, B. Yang2, and A. Fitzsimmons3 1 Planetary and Space Sciences, School of Physical Sciences, The Open University, Milton Keynes, MK7 6AA, UK e-mail: [email protected] 2 European Southern Observatory, Alonso de Cordova 3107, Vitacura, Casilla 19001, Santiago, Chile 3 Astrophysics Research Centre, School of Mathematics and Physics, Queen’s University Belfast, Belfast, BT7 1NN, UK Received 28 April 2017 / Accepted 17 June 2017 ABSTRACT Context. Main belt comets are a recently identified population of minor bodies with stable asteroid-like orbits but cometary appear- ances. Sublimation of water ice is the most likely mechanism for their recurrent activity (i.e. dust tails and dust comae), although there has been no direct detection of gas. These peculiar objects could hold the key to the origin of water on Earth. Aims. In this paper we present a search for the gas responsible for lifting dust from P/2012 T1 (Pan-STARRS), and review previous attempts at such measurements. To date such searches have mainly been indirect, looking for the common cometary gas CN rather than gasses related to water itself. Methods. We use the VLT and X-shooter to search for emission from OH in the UV, a direct dissociation product of water. Results. We do not detect any emission lines, and place an upper limit on water production rate from P/2012 T1 of 8−9 × 1025 molecules s−1.
    [Show full text]
  • Starscan Johnson Space Center Astronomical Society VOLUME 22, NUMBER 6 June 2006
    Starscan Johnson Space Center Astronomical Society VOLUME 22, NUMBER 6 June 2006 IN THIS ISSUE Top Stories and Special Interest Reports 3 — Visual Observing 5 — 2006 Star Party Dates 6 — Ed Morrison 6 — Asteroid 16020 Tevelde 7 — Living Astronomy History 8 — The Pearline Maiden in the Moon 19 — Interesting Website 20 — Mercury Transit 21 — Member’s Gallery In the News 9 — New Milky Way Companions Found 10 — Site in Chile Selected for Large Synoptic Survey Telescope 11 — NASA and Partners Release New Movies of Titan 12 — JPL Slide Show: The Infrared Universe 13 — Spitzer Telescope Sees Trail of Comet Crumbs 14 — Astronomers Use Innovative Technique to Find Extrasolar Planet 16— Astronomer Wins Top Prize For Creating Black Hole Web Site Club News and Information 17 — Upcoming Events 19 — Magazine Subscriptions 19 — Houston Area Astronomy Clubs 20 — IDA News 20 — For Sale 23 — Next Meeting 23 — Officers 23 — Agenda 23 — Starscan Submissions 23 — Cover Image Visual Observing June 2006 SSO: (Solar System Objects) Summary for the 15 June 06 Object Const Mag % Rise Time Transit Set Time Ill Sun Tau -26.7 100 06:20 13:20 20:21 Moon Cap ---- 78 00:00 04:51 10:11 Mercury Gemi 0.2 48 08:09 15:08 22:11 Venus Ari -3.9 81 04:20 10:59 17:39 Mars Cnc 1.8 96 09:36 16:25 23:17 Jupiter Lib -2.4 100 16:43 22:17 03:48 Saturn Cnc 0.8 100 09:42 16:29 23:19 Uranus Aqr 5.8 100 01:04 06:51 12:37 Neptune Cap 7.9 100 23:48 05:14 10:41 Pluto Ser 13.9 99 20:03 01:28 06:53 Schwassmann- Cet 9.1 46 03:41 09:18 14:55 Wachmann 73P Honda-Mrkos- Tau 9.7 84 04:49 11:34 18:18 Pajdusakova 45P Highlighted times denote daylight events.
    [Show full text]
  • Abstract: Comet Dust Is Primitive and Shows Significant Diversity. Our Knowledge
    Abstract: Comet dust is primitive and shows significant diversity. Our knowledge of the properties of primitive particles has expanded significantly through microscale investigations of cosmic dust samples (IDPs and AMMs) and of comet dust samples (Stardust and Rosetta's COSIMA), as well as through remote sensing (spectroscopy and imaging) via Spitzer and via spacecraft encounters with 103P/Hartley 2 and 67P/Churyumov-Gerasimenko. Microscale investigations show that comet dust and cosmic dust are particles of unequilibrated materials, including aggregates of materials unequilibrated at submicron scales. We call unequilibrated materials "primitive" and we deduce they were incorporated into ice-rich (H2O- , CO2-, and CO-ice) parent bodies that remained cold, i.e., into comets, because of the lack of aqueous or thermal alteration since particle aggregation; yet some Stardust olivines suggest mild thermal metamorphism. Primitive particles exhibit a diverse range of: structure and typology; size and size distribution of constituents; concentration and form of carbonaceous and organic matter; D-, N-, and O- isotopic enhancements over solar; Mg-, Fe-contents of the silicate minerals; the compositions and concentrations of sulfides, and of less abundant mineral species such as chondrules, CAIs and carbonates. The unifomity within a group of samples points to: aerodynamic sorting of particles and/or particle constituents; the inclusion of a limited range of oxygen fugacities; the inclusion or exclusion of chondrules; a selection of organics. The properites of primitive particles imply there were disk processes that resulted in different comets having particular selections of primitive materials. The diversity of primitive particles has implications for the diversity of materials in the protoplanetary disk present at the time and in the region where the comets formed.
    [Show full text]
  • The Astronews July 2021
    The Astronews www.hawastsoc.org July 2021 A word from your editor by Inside this issue: Sapavith ‘Ort’ Vanapruks HAS have decided to cancel public HAS Club Information 2 events for the time being for both public star party at Dillingham and in town star parties President’s Message 2 at Kahala and Geiger, as well as the monthly club meeting. These cancellations will con- tinue while we are still in tier level. As we Observer’s Notebook 3 are now in modified tier 4 on Oahu, we will only have the club member only star party. We will be limiting the club party to the key Meeting Minutes 4 master and 29 extra members. Please check your email and website for an update. Event Calendar 5 I have been trying to capture ISS transit in front of the Sun/Moon for many years. I used ISS Transit Finder website (https:// NASA’s Night Sky Notes 7 transit-finder.com/) to help me find the trans- it near me. Those many times I tried, I failed due to many reasons. Some of the reasons Meteor Log 8 are bad weather, incorrect camera setting, and unstable mount. Treasurer’s Report 9 Upcoming Events: • The next Board meeting is Sun., July 4th 3:30 PM. (Zoom Meeting) • The next meeting is on Tue., July 6th at the Bishop Museum at 7:30 PM. —Zoom Meeting • Bishop Museum’s planetarium shows are every 1st Saturday of the month at 8:00 PM (Online) www.bishopmuseum.org/calendar The latest opportunity was this past Tues- day morning, 6/29/2021, at 1:27 AM.
    [Show full text]